[1]Schnitzer M.Soil organic matter-the next 75 years[J].Soil Science,1991,151(1):41-58. [2]骆东奇,白洁,谢德伦.论土壤肥力评价指标和方法[J].土壤与环境,2002,11(2):202-205. [3]Hernanz J L,López R,Navarrete L,et al.Long-term effects of tillage systems and rotations on soil structural stability and organic carbon stratification in structural stability and organic carbon stratification in semiarid central Spain[J].Soil and Tillage Research,2002,66(2):129-141. [4]Vergnoux A,Guiliano M,Dirocco R,et al.Quantitative and mid-infrared changes of humic substances from burned soils[J].Environmental Research,2010,111(2):205-214. [5]梁尧,韩晓增,丁丽雪.东北黑土有机质组分与结构的研究进展[J].土壤,2012,44(6):888-897. [6]Canellas L P,SpacciniR,Piccolo A,et al.Relationships between chemical characteristics and root growth promotion of humicacids isolated from Brazilian Oxisols[J].Soil Science,2009,174 (11):611-620. [7]窦森,Yves Tardy,张晋京,等.土壤胡敏酸与富里酸热力学稳定性及其驱动因素初步研究[J].土壤学报,2010,47(1):71-76. [8]ShindoH,YoshidaM,YamamotoA,et al.δ13C values of organic constituents and possible source of humic substances in Japanese volcanic ash soils[J].Soil Science,2005,170 (3):175-182. [9]Ferrara G,LoffredoE,SenesiN.Anticlastogenic,antitoxic and sorption effects of humic substances on the mutagen maleic hydrazide tested in leguminous plants[J].European Journal of Soil Science,2004,55(3):449-458. [10] 邵帅,何红波,张威,等.土壤有机质形成与来源研究进展[J].吉林师范大学学报(自然科学报),2017,38(1):126-130. [11] 窦森,张晋京,Lichtfouse E,等.用δ13C方法研究玉米秸秆分解期间土壤有机质数量动态变化[J].土壤学报,2003,40(3):328-334. [12]郑利远,陈一民,焦晓光,等.长期施肥对不同有机质含量农田黑土活性有机氮组分的影响[J].中国农学通报,2016,32(5):96-100. [13]鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,1999:146-205. [14]窦森,于水强,张晋京.不同CO2浓度对玉米秸秆分解期间土壤腐殖质形成的影响[J].土壤学报,2007,44(3):458-466. [15]张晋京,宋祥云,窦森.连续提取对土壤腐殖质组分数量与特性的影响[J].土壤通报,2007,38(3):452-456. [16]李尚,许旭,陶巍,等.富里酸在土壤环境中的吸附研究[J].环境科学与管理,2015,40(3):78-81. [17]汤海明,肖保华.滴定分析法在土壤胡敏酸研究中的应用[J].地球与环境,2017,45(2):151-156. [18]张晋京,窦森.土壤胡敏素研究进展[J].生态学报,2008,28(3):1229-1239. [19]温延臣,李燕青,袁亮,等.长期不同施肥制度土壤肥力特征综合评价方法[J].农业工程学报,2015,31(7):91-98. [20]李凯,窦森,韩晓增,等.长期施肥对黑土团聚体中腐殖质物质组成的影响[J].土壤学报,2010,47(3):579-583.
|